Dew Point

Dew Point

Dew Point Temperature is a measure of humidity. If air is cooled eventually enough energy will be removed for water vapor to begin to condense. The temperature where condensation begins is the dew point temperature. If the air is gradually cooled while maintaining the moisture content constant, the relative humidity will rise until it reaches 100%. This temperature, at which the moisture content in the air will saturate the air, is called the dew point. If the air is cooled further, some of the moisture will condense.

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